Location of high-frequency P wave microseismic noise in the Pacific Ocean using multiple small aperture arrays
We investigate source locations of P wave microseisms within a narrow frequency band (0.67–1.33 Hz) that is significantly higher than the classic microseism band (~0.05–0.3 Hz). Employing a backprojection method, we analyze data recorded during January 2010 from five International Monitoring System...
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Veröffentlicht in: | Geophysical research letters 2015-04, Vol.42 (8), p.2700-2708 |
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